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CORRELATION BETWEEN CBR VALUE AND
UNDRAINED SHEAR STRENGTH FROM
VANE SHEAR TEST
NOOR ASMAH BINTI HUSSIN
A report submitted in partial fulfillment of the
requirements for the award of the degree of
Bachelor of Civil Engineering
Faculty of Civil Engineering
Universiti Teknologi Malaysia
APRIL, 2008
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I declare that this thesis entitled Correlatioan between CBR Value
and Undrained Shear Strength from Vane Shear Test is the result
of my own research except as cited in the references. The thesis
has not been accepted for any degree and is not concurrently
submitted in candidature of any other degree.
Signature :
Name : Noor Asmah Binti Hussin
Date : 28 April 2008
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TO MY BELOVED PARENTS, FAMILY AND FRIENDS
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ACKNOWLEDGEMENT
I would like to take this opportunity to express my special thanks firstly to my
supervisor, Prof. Dr. Khairul Anuar Bin Kassim, for spending his precious time to
supervise my research, always gives advices and invaluable guidance towards the
preparation of this thesis.
Secondly, I would like extend my thanks and appreciation to FKA Geotechnical
Lab technicians, FKA lecturers and staffs for their guidance and help to complete my
research. And also not to forget the supports and helps from all my friends and who ever
involved direct or indirectly in my research, thank you so much.
Last but not least, a thousand thanks to my beloved parents and my family,
without your love, caring and supports, I cant finish my final year thesis and also
complete my study in UTM.
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ABSTRACT
California Bearing Ratio (CBR) is a commonly used indirect method to
assess the stiffness modulus and shear strength of subgrade in pavement design works.
Over the years, many correlations had been proposed by various researchers. A study
was carried out to find the correlation between CBR values and undrained shear strength
for three types of soils. Correlation developed will be used as a basis for prediction.
Several soil samples with different PI and moisture content were compacted and tested
using CBR test and Vane shear test to obtain the data to establish the correlation. Based
on the results, a correlation had been proposed to predict the CBR values of the soil
sample for silty to clayey soil. These correlations were developed based on the
undrained shear strength from vane shear test. The established correlation from this
study covers only for Malaysian practices in predicting CBR values for subgrade.
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ABSTRAK
Nisbah Galas California (CBR) merupakan satu kaedah tidak langsung
untuk mengukur modulus kekerasan dan kekuatan ricih tanah bagi kerja-kerja
rekabentuk jalan raya berturap. Dalam beberapa tahun lalu, pelbagai korelasi telah
dicadangkan oleh ramai penyelidik. Satu penyelidikan telah dijalankan untuk
mendapatkan korelasi antara nilai CBR dengan kekuatan ricih tanah tak bersalir daripada
ujian ricih Vane (Vane shear test) untuk tiga jenis tanah. Korelasi yang telah diterbitkan
akan digunakan sebagai asas ramalan. Beberapa jenis tanah dengan indeks keplastikan
dan kandungan air berbeza dipadatkan dan diuji menggunakan ujian CBR dan ujian ricih
Vane untuk mendapatkan data-data yang diperlukan untuk menerbitkan korelasi.
Merujuk kepada keputusan, satu korelasi telah di cadangkan untuk meramal nilai CBR
untuk sampel tanah dari jenis berkelodak hingga ke tanah liat. Korelasi ini diterbitkan
berdasarkan kekuatan ricih tak bersalir daripada ujian ricih Vane. Korelasi yang telah
diterbitkan daripada penyelidikan ini hanya sesuai untuk meramalkan nilai CBR untuk
jalan raya berturap di Malaysia.
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TABLE OF CONTENTS
CHAPTER TITLE PAGE
TITLE i
DECLARATION ii
DEDICATION iii
ACKNOWLEDGEMENT iv
ABSTRACT v
ABSTRAK vi
TABLE OF CONTENTS vii
LIST OF TABLES x
LIST OF FIGURES xi
LIST OF SYMBOLS xii
LIST OF APPENDICES xiii
1 INTRODUCTION
1.1 BACKGROUND OF STUDY 1
1.2 PROBLEM STATEMENT 2
1.3 OBJECTIVES OF RESEARCH 3
1.4 SCOPE OF RESEARCH 3
1.5 SIGNIFICANCE OF RESEARCH 4
2 LITERATURE REVIEW
2.1 COHESIVE SOIL 5
2.2 SHEAR STRENGTH OF COHESIVE SOIL 5
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2.3 UNDRAINED SHEAR STRENGTH 7
2.3.1 UNCONFINED COMPRESSION
TEST 8
2.3.3 VANE SHEAR TEST 8
2.3.4 SENSITIVITY 9
2.3.5 CONSISTENCY 9
2.4 VANE SHEAR TEST 10
2.4.1 THEORY 11
2.4.2 APPARATUS 13
2.4.3 DERIVATION OF EQUATION 13
2.5 CALIFORNIA BEARING RATIO TEST 14
2.5.1 APPLICATIONS OF CBR 16
2.5.2 APPARATUS 17
2.5.3 ROAD PAVEMENT DESIGN
MANUALS 18
3 RESEARCH METHODOLOGY
3.1 INTRODUCTION 20
3.2 COLLECTION OF SAMPLE 20
3.3 SOIL PRELIMINARY TESTING 21
3.4 SOIL SELECTION 21
3.5 PREPARATION OF REMOULDED
SAMPLING 22
3.6 LABORATORY SOIL TESTING 23
3.7 DATA COLLECTION 23
3.8 DATA ANALYSIS 23
4 EXPERIMENTAL PROGRAM
4.1 STANDARD COMPACTION 27
4.2 VANE SHEAR TEST 30
4.3 CBR TEST 32
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5 RESULTS AND ANALYSIS
5.1 TYPICAL RANGE OF CBR VALUE 31
5.2 UNDRAINED SHEAR STRENGTH AND
AVERAGE CBR VALUE FOR SOIL
SAMPLE WITH DIFFERENT PI
AND MOISTURE
CONTENT 37
5.3 CBR VALUE VERSUS PLASTIC INDEX
OVER MOISTURE CONTENT 40
5.4 UNDRAINED SHEAR STRENGTH
VERSUS PLASTIC INDEX OVER
MOISTURE CONTENT 41
5.5 CORRELATION OF CBR VALUE
VERSUS UNDRAINED SHEAR
STRENGTH 42
6 CONCLUSIONS AND RECOMMENDATIONS
6.1 CONCLUSIONS 44
6.2 RECOMMENDATIONS 46
REFERENCES 47
APPENDICES 48
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LIST OF TABLES
TABLE NO. TITLE PAGE
2.1 Values of undrained shear strength versus
consistency 10
2.2 CBRs for commonly subgrade conditions 19
5.1 CBR value for marine clay 34
5.2 CBR value for white clay 35
5.3 CBR value for white kaolin 36
5.4 Undrained shear strength and average
CBR value of all sample tested. 38
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LIST OF FIGURES
FIGURE NO. TITLE PAGE
2.1 Four thin rectangular blades 11
2.2 Sample of soil 12
2.3 Stress distribution on blades 13
2.4 CBR test apparatus 18
3.1 Flowchart of Research Methodology 25
3.2 Preparation of Remoulded Sample Flowchart 26
4.1 Compaction Apparatus 27
4.2 Compaction in CBR mould 29
4.3 Hand held vane shear test 31
4.4 Vaneborer 31
5.1 CBR test graph for marine clay 20% moisture 35
content
5.2 CBR test graph for white clay 30% moisture content 36
5.3 CBR test graph for white kaolin 35% moisture
Content 37
5.4 Graph of CBR value versus plastic index over
moisture content 40
5.5 Graph of Undrained shear strength versus
plastic index over moisture content 41
5.6 Graph correlation of CBR value versus
undrained shear strength from vane shear test 42
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LIST OF SYMBOLS
A - Clay Activity
CBR - California Bearing Ratio
CBRBOTTOM - CBR value at bottom face of soil sample
CBRTOP - CBR value at top face of soil sample
D - Diameter of vane
H - Height of vane
LL - Liquid Limit
MDD - Maximum Dry density
OMC - Optimum Moisture content
PI - Plastic Index
tS - Sensitivity
us - Undrained shear strength
T - Applied torque
VST - Vane shear test
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LIST OF APPENDICES
APPENDIX TITLE PAGE
A Data for compaction test 48
B Data for vane shear test 57
C Data for CBR test 63
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CHAPTER 1
INTRODUCTION
1.1 Background of Study
Geotechnical engineering has been critical to highway construction since
engineers realized that successful civil works depended on the strength and integrity of
the foundation material. Road design and construction over soft ground especially over
very soft and soft marine deposits are interesting engineering challenges to engineers
especially at the approaches to bridges and culverts. Many geotechnical options are
available for engineers consideration. Very soft and soft deposits of river alluvium and
marine deposits are common in Southeast Asia. The river alluvium and marine deposits
normally consist of clay, silty clay and occasionally with intermittent of sand lenses
especially near a major river mouth and delta. The marine deposits in Malaysia are
encountered along the coast of the Peninsular, where they are up to 20km in width.
Embankment design of roads needs to satisfy two important requirements among
others; the stability and settlement. The short term stability for embankment over soft
clay is always more critical than long term simply because the subsoil consolidates with
time under loading and the strength increases. In design, it is very important to check for
the stability of the embankment with consideration for different potential failure surfaces
namely circular and noncircular. It is also necessary to evaluate both the magnitude and
rate of settlement of the subsoil supporting the embankment when designing the
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embankment so that the settlement in the long term will not influence the serviceability
and safety of the embankment.
Very often, the non-circular failure is more critical than circular slip failure for
layered soil especially with very soft subsoil at top few meters. Long term stability of
embankment is usually not an issue for embankment over soft marine deposits because
the subsoil would gain strength with time after the excess pore water pressure in the
subsoil dissipates during consolidation. When the analyses based on subsoil and
thickness of embankment indicate multistage construction is required, the construction
of the embankment usually take substantially longer time especially when the cohesive
subsoil does not have sand lenses. However, geometry change requires wide road
reserve due to flatter slope and stabilizing berms. It has been shown that geotechnical
design can be innovative solutions for highway construction problems.
1.2 Problem Statement
Nowadays in Malaysia, there are so many constructions of highways. Since
highways also involve foundation, these means geotechnical aspects are also important
in the highway construction. Shear strength parameters are always associated with the
bearing capacity of the soil. However for highway engineers, they always prefer to use
CBR test to determine the suitable strength for designing road pavement. This research
is to find the correlation between CBR and undrained shear strength of subgrade. It can
provide better understanding between highway and geotechnical engineer.
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1.3 Objectives of Research
The aim of the research is to close gap between how to relate CBR and shear
strength of soil in undrained shear strength aspect. The specific objectives of the
research are:
To determine the CBR and undrained shear strength for soil with different
PI and different types of soil.
To establish CBR and undrained shear strength from vane shear of soil
samples at different moisture content.
To establish the correlation between CBR value and undrained shear
strength from vane shear test.
1.4 Scope of Research
The sample used in this research only involved soils from Johor Bahru areas. The
data used in this research are of marine clay, white Kaolin and white clay with different
Plastic Index. The samples for this research are based on compaction sample. The shear
strength obtained from this research are from vane shear test and only limit for silty to
clayey soil since vane shear test is typically performed on soft, saturated cohesive soils.
The correlation in this research covers only for Malaysian practices in predicting CBR
values for subgrade.
.
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1.5 Significance of Research
This research will narrow the gap of understanding on soil strength for the
geotechnical and highway engineers. Since these two different disciplines in civil
engineering have their own understanding on the use of soil parameters in design, it is
appropriate to establish some basis for interpretation of CBR in terms of shear strength
parameter and vice versa.
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CHAPTER 2
LITERATURE REVIEW
2.1 Cohesive Soil
Cohesive soil is the type of soil that in small soil particle forms and has higher
water content. Cohesive soils consist of silts, clays and organic material. Clay are low
strength and high compressibility and many are sensitive. The clay is consisting of
several minerals. Silica Tetrahedron and Alumina Octahedrons are the basic units to
compose the clay minerals. The size of clay is very small, which is less than 2m and
electrochemically very active. Clay minerals are produced mainly from the chemical
weathering and decomposition of feldspars, such as Orthoclase and Plagioclase and
some Mica.
2.2 Shear Strength of Cohesive Soil
Soil can be classified as being either nonplastic or plastic. The shear strength of
nonplastic soils known as cohesionless soils or granular soils. The shear strength of
plastic soils, known as cohesive soils. Cohesive soils have fines, which are silt and clay
size particles that give the soil a plasticity or ability to be moulded and rolled. Typical
types of cohesive soils are silts and clays. The shear strength of cohesive soil is much
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more complicated than the shear strength of cohesionless soils. Also, in general the shear
strengths of cohesive soil tend to be lower than the shear strengths of cohessionless soils.
As a result, more shear induced failures occur in cohesive soils, such as clays, than in
cohesionless soils.
The shear strength of cohesive soil can generally be divided into three broad groups:
1. Undrained shear strength
This is also known as the shear strength based on a total stress analysis. The
purpose of these laboratory tests is to obtain either the undrained shear strength
of the soil or the failure envelope in terms of total stresses. These types of shear
strength tests are often referred to undrained shear strength tests because there is
no change in water content of the soil during the shear portion of the test.
2. Drained shear strength
This is also known as the shear strength of soil based on an effective stress
analysis. The purpose of these laboratory tests is to obtain the effective shear
strength of the based on the failure envelope in terms of effective stress. These
types of shear strength tests are often referred to as drained shear strength tests
because the water content of the soil is allowed to change during shearing.
3. Drained residual shear strength
For some projects, it may be important to obtain the residual shear strength of
cohesive soil, which is defined as the remaining shear strength after a
considerable amount of shear deformation has occurred. The drained residual
shear strength can be applicable to many types of soil conditions where a
considerable amount of shear deformation has already occurred.
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In summary, the basic types of laboratory shear strength tests for cohesive
soils are as follows:
Unconsolidated undrained (UU)
Consolidated undrained (CU)
Consolidated undrained with pore water pressure measurements
(CU)
Consolidated drained (CD)
Drained residual shear strength
2.3 Undrained Shear Strength us
As the name implies, the undrained shear strength us refers to a shear condition
where water does not enter or leave the cohesive soil during the shearing process. In
essence, the water content of the soil must remain constant during the shearing process.
There are many projects where the undrained shear strength is used in the design
analysis. In general, these field situations must involve loading or unloading of the
cohesive soil at a rate that is much faster than the shear-induced pore water pressures can
dissipate.
During rapid loading of saturated cohesive soils, the shear-induced pore water
pressure can only dissipate by the flow of water into (negative shear-induced pore water
pressures) or out of (positive shear-induced pore water pressures) the soil. Cohesive soil
has a low permealibility, and if the load is applied quickly enough, there will not be
enough time for water to enter or leave the cohesive soil. For such a quick loading
condition of a saturated cohesive soil, the undrained shear strength us should be used in
analysis.
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2.3.1 Unconfined compression test
The unconfined compression test is a very simple type of test that consists of
applying a vertical compressive pressure to a cylinder of laterally unconfined cohesive
soil. The unconfined compression test is also known as a simple compression test.
The unconfined compression test is most frequently performed on cohesive soils
that are in a saturated condition, such as soil obtained from below the groundwater table.
Because the soil specimen is laterally unconfined during testing, the soil specimen must
be able to retain its plasticity during the application of the vertical pressure. In addition,
the soil must not expel water during the compression test. For these reasons, the
unconfined compression test is most frequently performed on saturated clays. Soils that
tend to crumble, fall apart, or bleed water during the application of the vertical pressure
should not be tested.
2.3.3 Vane shear test
Vane shear test also can be used to obtain the undrained shear strength us of
cohesive soil. The vane test is typically performed on soft, saturated cohesive soils, such
as clays located below the groundwater table. The vane shear test basically consists of
inserting a four blade vane into the cohesive soil and then rotating the vane to determine
the torsional force required to shear the cohesive soil is then converted to the undrained
shear resistance of the cylindrical surface.
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2.3.4 Sensitivity
The unconfined compressive test and the vane shear test can be performed on
completely remolded soil specimens in order to determine the sensitivity tS is defined as
the undrained shear strength us of an undisturbed soil specimen divided by the
undrained shear strength us of a remolded soil specimen. Based on the sensitivity, the
cohensive soil can be classified as having a low, medium, high, or quick sensitivity.
When a remolded soil specimen is tested, it is important to retain the same water
content of the undisturbed soil. To accomplish this objective, the soil can be placed in a
plastic bag and then thoroughly remolded by continuously squeezing and deforming the
soil. If the soil specimen bleeds water during this process, then the sensitivity cannot be
determined for the soil. After remolding, the soil is carefully pressed down into a mold,
without trapping any air within the soil specimen. Once extruded from the mold, the
remolded soil is ready for testing.
2.3.5 Consistency
The unconfined compressive test and the vane shear test can also be used to
determine the consistency of cohesive soil. The consistency is also known as the degree
of firmness of the soil. Based on the undrained shear strength us of an undisturbed
specimen, cohesive soils are deemed to have a very soft, soft, medium, stiff, very stiff, or
hard consistency. The values of undrained shear strength versus consistency are listed
below:
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Table 2.1 : Values of undrained shear strength versus consistency
Cohesive soil consistency Undrained shear strength, kPa Undrained shear strength, psf
Very soft us < 12 us < 250
Soft 12 us < 25 250 us < 500
Medium 25 us < 50 500 us < 1000
Stiff 50 us < 100 1000 us < 2000
Very stiff 100 us < 200 2000 us < 4000
Hard us 200 us 4000
2.4 Vane Shear Test
Vane Shear Test is one of the oldest and most widely used methods where
developed and investigated extensively in Sweden from late 1940s. Similar to the
unconfined compression test, the vane shear test is another type of test that can be used
to obtain the undrained shear strength us of cohesive soil in accordance to BS 1377 : Part
9 : 1980. The vane shear test is typically performed on undisturbed samples and samples
prepared by the standard-compaction procedures.
The structural strength of soil is basically a problem of shear strength. Vane
shear test is a useful method of measuring the shear strength of clay. It is cheaper and
quicker. The laboratory vane shear test for the measurement of shear strength of
cohesive soils is useful for soils of low shear strength (less than 0.3 kg/cm) for which
triaxial or unconfined tests cannot be performed. The undisturbed and remolded strength
obtained are useful for evaluating the sensitivity of soil.
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The vane consists of four thin rectangular blades or wings welded to an
extendable circular rod. Generally the height of the vane is about twice of its width. The
vane is pushed into the soil for at least twice its height and is then rotated at a constant
rate of 0.1 to 0.2 degrees per second until the soil is ruptured. The maximum torque
required to shear the cohensive soil is then converted to the undrained shear resistance of
the cylindrical surface.
Figure 2.1 : Four thin rectangular blades
2.4.1 Theory
For the maximum torque, T need to rupture the soil along the surface area of the
cylinder, the shear strength at failure is computed by the following relationship.
T = Su
+
6
D
2
D 32
T
H
D Extendable rod
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where
T = applied torque
D, H = diameter and height of vane, respectively
su = undrained shear strength of soil
The equation assumes uniform stress distribution at both horizontal ends of the vane and
the vertical cylindrical surface with the diameter and height equal to that of the vane.
To compute the shear strength at the failure by the following relationship:
Figure 2.2 : Sample of soil
Where
T = applied torque
D, H = diameter and height of vane, respectively
Su = undrained shear strength of soil
T = Su (D2H/2 + D
3/6)
Su = T/ (D2H/2 + D
3/6)
D
H
r
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2.4.2 Apparatus
1. Vane shear apparatus - four thin rectangular blades or wings welded to an
extendable circular rod.
2. 4 springs with different elastic coefficients.
2.4.3 Derivation of equation
Figure 2.3 : Stress distribution on blades
Assumed that the soils resistance to shear is equivalent to a uniform shear stress, equal
to the undrained strength of soil, su , and acting on both the perimeter and the ends of the
cylinder.
H
D
Assumed stress
distribution on blades
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End torque = 2 su r
0
2 r2 dr with r = D / 2
= 2 su [2 r3 / 3 ]
r
0
= 2 su [2 r3 / 3 ] 2/0
D
= 2 su [2 D3/8
1/3 ]
= [su D3]/ 6
Side torque = su D H D / 2
= [su D2 H ] / 2
The maximum torque, T = [su D2 H ] / 2 + [su D
3]/ 6
= su (D2 H / 2 + D
3 / 6 )
2.5 California Bearing Ratio Test
The California Bearing Ratio (CBR), was developed by The California State
Highways Department. It is in essence a simple penetration test to developed and
evaluate the strength of road subgrades. The strength of the subgrade is the main factor
in determining the thickness of the pavement. The value of the stiffness of the subgrade
is required if the stresses and strains in pavement and subgrade are to be calculated. The
CBR is a comparative measure of the shearing resistance of a soil. It is used in the
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design of asphalt pavement structures. This test consists of measure the load required to
cause a plunger of standard size to penetrate a soil specimen at a specified rate. The CBR
is the load, in megapascals required to force a piston into the soil a certain depth,
expressed as a percentage of the load, in megapascals, required to force the piston the
same depth into a standard sample of crushed stone. Usually depths of 2.5 or 5.0 mm are
used, but depth of 7.5, 10 and 12.5 mm may be used if desired. Penetration loads for the
crushed stone have been standardized. The resulting bearing value is known as the
California Bearing Ratio, which generally abbreviated to CBR, with the percent omitted.
Generally, the CBR value for a soil will depend upon its density, molding
moisture content, and moisture content after soaking. Since the product of laboratory
compaction should closely represent the result of field compaction, the first two of these
variables must be carefully controlled during the preparation of laboratory sample for
testing. Unless it can be moisture and be affected by it in the field after construction, the
CBR tests should be performed on soaked sample. It sounds complicated, but the basis
behind it is quiet simple. The resistance of the subgrade were determine to deformation
under the load from vehicle wheels. The CBR test is a way of putting a figure on this
inherent strength, the test is done in a standard manner so the strengths of different
subgrade materials can be compared and these figure can be used as a means of
designing the road pavement required for a particular strength of subgrade. The stronger
the subgrade (the higher the CBR reading) the less thick it is necessary to design and
construct the road pavement, this gives a considerable cost saving. Conversely if CBR
testing indicates the subgrade is weak, a suitable thicker road pavement must be
construct to spread the wheel load over a greater area of the weak subgrade in order that
the weak subgrade material is not deformed, causing the road pavement to fail.
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2.5.1 Applications of CBR
The main application of California Bearing Ratio (CBR) is to evaluate the
stiffness modulus and shear strength of subrade. Generally, the subgrade soil cannot bear
the construction and commercial traffic without any distress, therefore; a layer of rigid or
flexible pavement is required to be laid on top of the subgrade to carry the traffic load.
The determination of the thickness of the pavement layer is governed by the
strength of subgrade, thus the information on stiffnes modulus and shear strength of
subgrade are required before any pavement design is carried out. These parameters are
necessary to determine the thickness of the overlaying pavement n order to achieve
optimum and economic design. This stiffness modulus and shear strength of subgrade
are controlled by particularly plasticity, soil type, density, degree of remoulding and
effective stress (The Highway Agency, 1994). The effective stress is dependent on the
stress from the overlying soil layers, the stress history and the suction. In turn, suction is
depends on the moisture content history, soil types and depth of water table.
Due to the number of factors that make the measurement of stiffness modulus
and shear strength of subgrade complicated, it is necessary to adopt a more simplified
test method that can be used as an index test. The CBR test is a simple strength test that
compares the bearing capacity of a material with that of a well graded standard crushed
stone base material. This means that the standard crushed stone material should have a
CBR value of 100%. The resistance of the crushed stone under standardised conditions
is well established. Therefore, the purpose of a CBR test is to determine the relative
resistance of the subgrade material under the same conditions.
If the CBR value of subgrade is high, it means that the subgrade is strong.
Accordingly, the design of pavement thickness can be reduced in conjunction with the
stronger subgrade. Thus it will give a considerable cost saving in term of construction
besides an optimum design. However, if the CBR value of subgrade is weak with low
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CBR value, the thickness of pavement shall be increased in order to spread the traffic
load over a greater area of the weak subgrade. This is important to prevent the weak
subgrade material to deform excessively and causing the road pavement fail.
The CBR test is used exclusively n conjunction with pavement design methods
and the method of sample preparation and testing must relate to the assumptions made in
the design method as well as to assumed site conditions. For instance, the design may
assume that soaked CBR value are always used, regardless of actual site conditions
(Carter and Bentley, 1991)
2.5.2 Apparatus
1. 20mm BS test sieve
2. A balance capable of weighing up to 25kg readable and accurate to 5g.
3. A cylinder CBR mould having an internal diameter of 25mm and an
internal effective height of 127mm with detachable base plate and a collar
of 50mm deep.
4. Wooden hammer or rubble mallet
5. 4.5kg metal hammer
6. Spatula
7. Apparatus for moisture content determination.
8. CBR machine for applying the test forces through the plunger, consisting
of a force measuring device and means for applying the forces at a
controlled rate.
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Figure 2.4 : CBR test apparatus
2.5.3 Road Pavement Design Manuals and Publications Using CBR Values
The CBR in spite of its limited accuracy still remains the most generally accepted
method of determining subgrade strength, and as such this information, along with
information on traffic flows and traffic growth is used to design road pavements. The
"Transport and Road Research Laboratory Report 1132: The Structural Design of
Bituminous Roads", is the current basic design document for road pavements involving
highly trafficked roads i.e. mainly motorway and trunk roads. Recently published
excellent documents on road foundation/design and including CBR information are:
D.Tp. DESIGN MANUAL HD 25/94, ROAD FOUNDATIONS
D.Tp. DESIGN MANUAL HD 26/94, ROAD PAVEMENT DESIGN.
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Also some authorities have their own design documents giving minimum
highway pavement construction requirements for housing/industrial estate roads in
relation to CBR results. It is impossible to summarize the mentioned documents in
limited space, but you will find in them, graphs relating sub-base and road base
thickness to CBR values and cumulative traffic (in million standard axles, m.s.a.'s). Also
information on other methods of obtaining CBR results, which differ to the basic test,
described above is included in some of these publications.
This table is only for guidance; you should refer to a design document for
specific information.
Table 2.2 : CBRs for commonly subgrade conditions
CBR VALUE SUBGRADE
STRENGTH
COMMENTS
3% and less Poor Capping is required
3% - 5% Normal Widely encountered CBR
range capping considered
According to road category
5% - 15% Good Capping normally
unnecessary except on very
heavily trafficked roads.
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CHAPTER 3
RESEARCH METHODOLOGY
3.1 Introduction
This chapter discusses the methodology of the research. The process starts from
identifying the research topic, literature review, laboratory soil testing, data collection,
data analysis and finally the expected finding.
3.2 Collection of Sample
The soil sample used in this research involved three types of soil which are
marine clay, UTM white clay and White Kaolin with different Plastic Index. All the
samples are taken from Johor Bahru areas. They should be taken in such a way that they
have not lost fractions of the in situ soil (for example, coarse or fine particles) and,
where strength and compressibility tests are planned, they should be subject to as little
disturbance as possible.
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3.3 Soil Preliminary Testing
It is relevant for the samples to required index, classification and compaction
testing. Index tests are the basic and simplest types of laboratory tests performed on soil
samples. Index tests are used to determine the physical properties of the soil. Index tests
can be used to determine phase relationships, soil classification, or special index
properties. The tests performed in the laboratory includes water content, unit weight,
specific gravity test, relative density, particle size distribution and Atterberg limits.
Compaction is a physical process of getting the soil into a dense state can increase the
shear strength, decrease the compressibility, and decrease the permeability of the soil.
There are four basic factors that affect compaction which are soil types, material
gradation, water content and compaction effort.
3.4 Soil Selection
The availability of good engineering parameters for geotechnical design depends
on careful testing. Testing may be carried out in the laboratory or in the field, but in
either case the most important factor controlling the quality of the end result is likely to
be the avoidance of soil disturbance. Soil disturbance can occur during drilling, during
sampling, during transportation and storage, or during preparation for testing. Any
sample of soil being taken from the ground, transferred to the laboratory, and prepared
for testing will be subject to disturbance. The mechanisms associated with this
disturbance can be classified as follows:
1. Changes in stress conditions;
2. Mechanical deformation;
3. Changes in water content and voids ratio; and
4. Chemical changes.
-
Therefore, soil selection is very important to get the best result for this research.
Since this research needs sample with different Plastic Index, so samples with different
Plastic index in range of 10 to 50 will be selected.
3.5 Preparation of Remoulded Sampling
Prepare the remoulded specimen at maximum dry density or any other density at
which the research required. Compaction is the process of reducing the air ontent by the
application of energy to the moist soil. Compaction increases the number of particles
within a specific volume thereby increasing the shear strength. There are two ways to
prepare the specimen either by dynamic compaction or by static compaction:
Dynamic compaction
Compact the sample in the mould using either light compaction or heavy compaction.
For standard compaction, compact the soil in 3 equal layers, each layer being given 27
blows by the 2.5 kg hammer for compaction mould and 62 blows by the 4.5 kg hammer
for CBR mould. For modify compaction, compact the soil in 5 layers, each layer being
given 27 blows by the 2.5 kg hammer for compaction mould and 62 blows to each layer
by the 4.5 kg hammer for CBR mould.
Static compaction
The sample placed in the CBR mould with a filter paper and the displacer disc on the top
of soil. Keep the mould assembly in static loading frame and compact by pressing the
displacer disc till the level of disc reaches the top of the mould. Different pressure or
load apply to the sample; will produce different moisture content and density of the
sample.
-
3.6 Laboratory Soil Testing
The soil testing for this research involved three types of soil which are marine
clay, UTM white clay and White kaolin with different Plastic Index. Each types of soil
will divided to four different moisture contents which now produce twelve soil samples
for testing. Since water content is one of the important physical properties of soil
strength. Then, CBR test and vane shear test will conduct to these twelve samples of soil
to give 24 data to establish the correlation graph between CBR value and undrained
shear strength from vane shear test.
3.7 Data Collection
Data are collected from the laboratory soil testing which conducted as stated
above. A total number of 24 soil data from the tests used for this research. Adequate data
is important for carrying out the required analyses in order to achieve the objectives of
the research. This research involved nine sample of soil with different types, Plastic
Index and moisture content because many data are needed to correlate CBR value and
undrained shear strength from vane shear test.
3.8 Data Analysis
In order to meet the expected findings, detailed analysis need to be carried out on
the collected data based on various pressure, moisture content and density of the sample.
The data is calculated and analyzed by means of graphical and correlation method as
well as statistical functions integrated in Microsoft Excel or manually. A relationship
between two or more variables can be obtained by correlation method. This method is
-
not an experimental but it is a mathematical technique for summarizing the data that
corresponding to more than one variables. Correlation developed will be used as a basis
for prediction. Therefore, this method will be adopted to establish the correlation for this
research.
-
Figure 3.1 : Flowchart of Research Methodology
SOIL PRELIMINARY TESTING
SOIL SAMPLE SELECTION
COLLECTION OF SAMPLE
PREPARATION OF REMOULDED SAMPLING:
DYNAMIC STANDARD COMPACTION (CBR MOULD)
CONDUCT CBR AND VANE SHEAR TEST
DATA COLLECTION AND DATA ANALYSIS
PROPOSED CORRELATION
-
CHAPTER 4
EXPERIMENTAL PROGRAM
4.1 Standard Compaction
Compaction of soil is the process by which the solid particles are packed more
closely together, usually by mechanical means, thereby increasing the dry density of the
soil. The dry density which can be achieved depends on the degree of compaction
applied and on the amount of water present in soil. For a given degree of compaction of
a given cohesive soil there is an optimum moisture content at which the dry density
obtained reaches a maximum value.
Figure 4.1: Compaction Apparatus
-
The compaction procedures are:
1. Determine the weight of the CBR mould + base plate (not the extension),
W1, (lb).
2. Attach the extension to the top of the mould.
3. Pour the moist soil into the mold in 3 equal layers. Each layer should be
compacted uniformly by the 2.5 kg hammer 62 blows before the next
layer of loose soil is poured into the mould.
7. Remove the top attachment from the mould. Be careful not to break off
any of the compacted soil inside the mould while removing the top
attachment.
8. Using a straight edge, trim the excess soil above the mould. Now the top
of the compacted soil will be even with the top of the mould.
9. Determine the weight of the mould + base plate + compacted moist soil
in the mold, W2 (lb).
10. Remove the base plate from the mold. Using a jack, extrude the
compacted soil cylinder from the mold.
11. Take a moisture can and determine its mass, W 3 (g).
12. From the moist soil extruded in Step 10, collect a moisture sample in the
moisture can (Step 11) and determine the mass of the can + moist soil,
W 4 (g).
13. Place the moisture can with the moist soil in the oven to dry to a constant
weight.
14. Break the rest of the compacted soil (to No.4 size) by hand and mix it
with the left- over moist soil in the pan. Add more water and mix it to
raise the moisture content by about 2%.
15. Repeat Steps 6 through 12. In this process, the weight of the mold + base
plate + moist soil (W2) will first increase with the increase in moisture
-
content and then de- crease. Continue the test until at least two
successive down readings are obtained.
16. Determine the mass of the moisture cans + soil samples, W 5 (g) (from
Step 13).
Figure 4.2: Compaction in CBR mould
4.2 Vane Shear Test
-
This method covers the measurement of the shear strength of a sample of soft to
firm cohesive soil without having to remove it from its container or sampling tube. The
sample therefore does not suffer disturbance due to preparation of a test specimen. The
method may be used for soils that are too soft or too sensitive to enable a satisfactory
compression test specimen to be prepared. The shear strength of the remoulded soil, and
hence the sensitivity, can also be determined. In this research, inspection vane tester, H-
60 was used with the size of four bladed vane of 16 x 32 mm and multiply readings with
2. this size of blade can measure shear strength of 0 to 200 kPa. The procedures are:
1. Connect required vane and extension rods to the inspection vane
instrument. While screwing the vane or rods to instrument hold onto the
lower part.
2. Push the vane into the compacted soil sample. Donot twist the inspection
vane during penetration.
3. Make sure the graduated scale is set to 0positions.
4. Turn handle clockwise. Turn as slow as possible with constant speed.
5. When the lower part follows the upper part around or even falls back,
failure and maximum shear strength is obtained in the clay at the vane.
6. Holding handle firmly, allow it to return to 0 position.
7. Note the reading on the graduated scale. Do not touch or in any way
disturb the position of the graduated ring till the reading is taken.
8. To measure the friction between clay and the extension rods: extension
rods and vane shaft without vane are pushed into the soil sample to the
depth required for shear force measurements. The friction value thus
obtained is used to evaluate the actual shear strength from the measured
shear strength.
-
Figure 4.3: Hand held vane shear test
Figure 4.4: Vaneborer
-
4.3 California Bearing Ratio Test
CBR test is to determine the relationship between force and penetration when a
cylindrical plunger of a standard cross-sectional area is made to penetrate the soil at a
given rate. At certain values of penetration ratio of the applied force to a standard force,
expressed as percentage, is defined as the California Bearing Ratio (CBR). The
penetration test procedures are:
1. Place the mould with baseplate containing the sample, with the top face
of the sample exposed, centrally on the lower platen of the testing
machine.
2. Place the appropriate annular surcharge discs on top of the sample.
3. Fit it into place the cylindrical plunger and force-measuring device
assembly with the face of the plunger resting on the surface of the
sample.
4. Apply a seating force to the plunger, depending on the epected CBR
value, as follows,
a. For CBR value up to 5% apply 10 N
b. For CBR value from 5% to 30%, apply 50 N
c. For CBR value above 30% apply 250 N
5. Record the reading of the force-measuring device as the initial zero
reading.
6. Secure the penetration dial gauge in position. Record its initial zero
reading.
7. Start the test so that the plunger penetrates the sample at a uniform rate of
1 0.2mm/min, and at the same instant start timer.
8. Record the readings of the force gauge at the intervals of penetration of
0.25 mm, to a total penetration not exceeding 7.5 mm
-
9. Carry out the test on base by repeating all the above procedures.
Figure 4.5: CBR test apparatus
-
CHAPTER 5
RESULTS AND ANALYSIS
5.1 Typical Range of CBR Value
The CBR values from the data had been obtained from the soil samples. For
purpose of analysis, these tables below showed the CBR values and example of CBR
test graph for each type of soil obtained from 12 samples of soil .
Table 5.1 : CBR value for marine clay
CBR values 20% moisture content 2.5mm 5.0mm
Top (%) 10.837 10.697
Bottom (%) 14.637 12.673
CBR values 23% moisture content 2.5mm 5.0mm
Top (%) 3.852 5.195
Bottom (%) 8.654 7.938
CBR values 26% moisture content 2.5mm 5.0mm
Top (%) 1.900 2.010
Bottom (%) 2.799 2.691
CBR values 30% moisture content 2.5mm 5.0mm
Top (%) 0.796 0.988
Bottom (%) 1.104 1.192
-
CBR TEST GRAPH
0.000
0.500
1.000
1.500
2.000
2.500
3.000
3.500
0.000 2.000 4.000 6.000 8.000
PENETRATION OF PLUNGER(mm)
FORCE OF PLUNGER(kN)
bottom top
Figure 5.1 : CBR test graph for marine clay 20% moisture content
Table 5.2 : CBR value for white clay
CBR values 30% moisture content 2.5mm 5.0mm
Top (%) 2.764 3.545
Bottom (%) 4.515 4.706
CBR values 33% moisture content 2.5mm 5.0mm
Top (%) 0.645 0.810
Bottom (%) 0.875 1.039
CBR values 36% moisture content 2.5mm 5.0mm
Top (%) 0.334 0.392
Bottom (%) 0.488 0.528
CBR values 40% moisture content 2.5mm 5.0mm
Top (%) 0.090 0.094
Bottom (%) 0.103 0.119
-
CBR TEST GRAPH
0.000
0.200
0.400
0.600
0.800
1.000
1.200
1.400
0.000 1.000 2.000 3.000 4.000 5.000 6.000 7.000 8.000
PENETRATION OF PLUNGER(mm)
FORCE OF PLUNGER(kN)
bottom top
Figure 5.2 : CBR test graph for white clay 30% moisture content
Table 5.3 : CBR value for white kaolin
CBR values 25% moisture content 2.5mm 5.0mm
Top (%) 0.745 0.877
Bottom (%) 1.027 1.431
CBR values 30% moisture content 2.5mm 5.0mm
Top (%) 0.387 0.609
Bottom (%) 0.677 0.737
CBR values 35% moisture content 2.5mm 5.0mm
Top (%) 0.483 0.497
Bottom (%) 0.532 0.609
CBR values 40% moisture content 2.5mm 5.0mm
Top (%) 0.077 0.128
Bottom (%) 0.154 0.196
-
CBR TEST GRAPH
0.000
0.050
0.100
0.150
0.200
0.000 2.000 4.000 6.000 8.000
PENETRATION OF PLUNGER(mm)
FORCE OF PLUNGER(kN)
bottom top
Figure 5.3 : CBR test graph for white kaolin 35% moisture content
5.2 Average CBR Value and Undrained Shear Strength for Soil Samples with
Different PI and Moisture Content
According to BS 1377(1990) Part 4, California Bearing Ratio (CBR) values can
be obtained from the top and bottom end of the soil sample and the values obtained shall
be indicated separately in the test report. As stated in BS, the CBR values shall be
reported as CBR value at top face (CBRTOP) and CBR value at bottom face
(CBRBOTTOM) in two significant values. But in this research, the average value of
CBRTOP and CBRBOTTOM is used since the results from the both end of the sample are
within 10% of the mean value.
Undrained shear strength determined using a vane that is inserted into soft
sediment and rotated until the sediment fails. The moisture contents choose for soil
-
samples are greater than the optimum moisture content of each soil until the moisture
content before the samples become slurry and cannot be compacted. Since vane shear
test is typically performed on soft, saturated cohesive soils. The soil samples for vane
shear test also compacted in CBR mould to get the same undrained shear strength with
the same moisture content for the CBR test samples. From the 24 soil samples had been
tested, the CBR value and undrained shear strength from vane shear test for soil with
different PI and different moisture content had been determined.
Table 5.4 : Undrained shear strength and average CBR value of all sample tested.
TYPE OF SOIL PLASTIC
INDEX
MOISTURE
CONTENT
(%)
UNDRAINED
SHEAR
STRENGTH
FROM VST
(kPa)
AVERAGE
CBR
VALUE
(%)
Marine Clay 17.5 20 146 12.74
Marine Clay 17.5 23 111 6.93
Marine Clay 17.5 27 76 2.41
Marine Clay 17.5 30 50 1.09
White Clay 26 30 100.5 4.13
White Clay 26 33 46 0.93
White Clay 26 37 30 0.46
White Clay 26 40 23.5 0.11
White Kaolin 14.5 25 98 1.15
White Kaolin 14.5 30 34 0.67
White Kaolin 14.5 35 12 0.55
White Kaolin 14.5 40 6 0.16
-
Table 5.4 summarizes the CBR values and undrained shear strengths for marine
clay, white clay and white kaolin based on the 24 soil tested data. As seen in the table,
all the plastic index of the soil are in the range of 10 to 50%. Where the plastic index for
marine clay is 17.5%, white clay is 26% and white kaolin is 14.5%. All the soil samples
were taken from Johor Bahru areas which marine clay is from, white clay from , and
White kaolin from Kahang, Johor. The undrained shear strength from vane shear test for
all samples was in the range of 6 to 146 kPa. Which white kaolin sample with the
moisture content of 40% have the lowest undrained shear strength and marine clay
samples with 20 % moisture content have the highest undrained shear strength.
Meanwhile, the average CBR value for all samples was in the range of 0.11% to 12.74%.
These results showed that plastic index and moisture content affected the shear
strength and CBR value of the soils. Three published graphs have been selected for
evaluation in the study. The graphs were CBR value versus plastic index over moisture
content, undrained shear strength versus plastic index over moisture content and
correlation between CBR value versus undrained shear strength.
-
5.3 CBR Value Versus Plastic Index Over Moisture Content
CBR VALUE VS (PI/MOISTURE CONTENT)
0
2
4
6
8
10
12
14
0.3 0.4 0.5 0.6 0.7 0.8 0.9 1
PI/MOISTURE CONTENT
CBR VALUE (%)
marine clay white kaolin white clay
Figure 5.4: Graph of CBR value versus plastic index over moisture content
Based on the figure 5.1, it can be seen that the CBR values are proportional to the
plastic index. Therefore, the CBR value will increase with the increasing of plastic
index. For example, these three different types of soil in the same moisture content of
30% showed different CBR value which marine clay is 1.09%, white clay is 4.13% and
white kaolin is 0.67%. So from this result known that plastic index affects the CBR
value where soil sample with higher plastic index also have the higher CBR value and
vice versa. Meanwhile, the CBR values are inversely proportional with the moisture
contents. The increasing of moisture content will decrease the CBR value. From the data
can be seen that in a type of oil sample, for example marine clay soil, the highest
moisture content will produced the lowest CBR value compared to the three other
samples with lower content of moisture.
-
5.4 Undrained Shear Strength Versus Plastic Index Over Moisture Content
SHEAR STRENGTH VS (PI/MOISTURE CONTENT)
0
20
40
60
80
100
120
140
160
0.3 0.4 0.5 0.6 0.7 0.8 0.9 1
PI/MOISTURE CONTENT
SHEAR STRENGTH(kPa)
Marine clay White kaolin White clay
Figure 5.5: Graph of Undrained shear strength versus plastic index over moisture
content
Figure 5.2 showed a graph which is almost similar to figure 5.1. Based on this
graph, the recorded range of undrained shear strengths are widely spread within 6 to 146
kPa which the difference for the highest and lowest strength is 140 kPa. The highest
undrained shear strength is from marine clay sample with 20% of misture content.
Meanwhile, white kaolin sample with 40% of moisture content produce the lowest
undrained shear strength out of the 24 samples. So we can conclude that, the undrained
shear strength of soil samples is also propotional with the plastic index. But the
undrained shear strength of soil samples is inversely proportional with the moisture
-
content. These mean, the undrained shear strength will decreases with the increasing of
moisture content in the soil.
5.5 Correlation Between CBR Value and Undrained Shear Strength
CBR VALUE VS UNDRAINED SHEAR STRENGTH
y = 0.0248x
R2 = 0.8027
y = 0.1212x - 7.0023
R2 = 0.7665
0
2
4
6
8
10
12
14
0 20 40 60 80 100 120 140 160
UNDRAINED SHEAR STRENGTH(kPa)
CBR V
ALUE(%
)
Figure 5.6: Graph correlation of CBR value versus undrained shear strength from
vane shear test
The plot of the CBR value against the undrained shear strength is presented in
Figure 5.3 based on the 24 soil data for three types of soft soils. Two best fit straight
-
lines were obtained from the plotted data as shown in the figure 1. The lines can be
represented by two linear equations as shown below:
1. For undrained shear strength in the range 0 73 kPa;
CBR value (average) = 0.0248x
2. For undrained shear strength in the range 73 146 kPa;
CBR value (average) = 0.1212x - 7.0023
Where; x = undrained shear strength
Based on the equation, CBR value can be predicted by knowing the value of undrained
shear strength or vice versa. It is observed that the average CBR value will be increase
with the increasing of undrained shear strength. As the CBR value can be correlated with
the undrained shear strength, it is a good indication that undrained shear strength can be
used to predict a CBR value for the soil.
-
CHAPTER 6
CONCLUSIONS AND RECOMMENDATIONS
6.1 CONCLUSIONS
Soil data had been obtained and analysed accordingly within the scope of the
study. All soil informations were obtained from laboratory tests accordance to British
Standard. Data acquired for analyses are from CBR values for top and bottom end of soil
samples, plastic index, moisture content and undrained shear strength from vane shear
test. Total soil data obtained was 24 numbers and three graphs have been made
according to certain circumstance and factors for evaluation in the study.
Based on the analyses carried out, the conclusion of the study can be summarized
as follow:
1. CBR value and undrained shear strength from vane shear test are
proportional with Plastic Index over moisture content. Therefore, CBR
value and undrained shear strength will increase with the increasing of
Plastic index over moisture content.
2. CBR value and undrained shear strength from vane shear test of soil
samples are inversely proportional with the moisture content. This mean,
-
CBR value and undrained shear strength will decrease with the increasing
of the moisture content.
3. The correlation between CBR value and undrained shear strength from
vane shear test had been established. From the correlation, CBR value can
be predicted using either one of these two linear equations depends on the
value of undrained shear strength :
i. Undrained shear strength in the range of 0 73 kPa:
CBR value (average) = 0.0248 x (undrained shear strength)
ii. Undrained shear strength in the range of 73 146 kPa:
CBR value (average) = 0.1212x (undrained shear strength) - 7.0023
4. The established correlation can close the gap between geotechnical and
highway engineer in undrained shear strength aspect for designing road
pavement in Malaysia.
-
6.2 RECOMMENDATIONS
Due to time constraints and limited soil data obtained for the soil samples, there
are some aspects which have not been covered in the study. Following are some
recommendations that can be carried out for future study or research in the subject of
correlation between CBR value and undrained shear strength from vane shear test:
1. The sample of soils used in this study are only limited to three types of
cohesionless soils which are marine clay, white clay and white kaolin. It
will be interesting to obtain more different types of soil such as Redish
brown clay, Light yellowish clay, etc for further study.
2. More data for soil samples should be obtained to evaluate a better
correlation. Since in this study, only 24 numbers of data obtained to
establish the correlation.
3. Establish the correlations using soil samples from other states in Malaysia
rather than Johor areas.
4. Correlate CBR value with undrained shear strength from other method
such as unconfined compression test. To compared which correlation is
more precise.
-
REFERENCES
1. British standards Institution (1990), Methods of Test for Civil Engineering
Purposes, London, BS 1377.
2. SAM 4062 Civil Engineering Laboratory II, Pejabat Akademik, Fakulti
Kejuruteraan Awam, UTM, 2003.
3. Soil Manual For The Design of Asphalt Pavement Structure, The Asphalt
Institute, USA, 1988.
4. Rodrigo Saldago, The Engineering of foundations, Purdue University.
5. C. R Scott(1980), An Introduction to Soil Mechanics and foundations,
Applied Science Publishers LTD, London.
6. P Purushothama Raj (1995), Geotechnical Engineering New Delhi Tata
McGraw Hill.
7. Terzaghi, K., Peck, R.B and Mesri, G. (1996) Soils Mechanics in Engineering
Practice. 3rd edition, United States of America: John Wiley & Sons, Inc.
-
APPENDIX A
Data for Compaction test
Marine Clay
PERCENTAGE 16%
MOULD(Kg) 3.692
MOULD + SOIL(Kg) 5.404
COMPACTED SAMPLE(Kg) 1.712
BULK DENSITY(Mg/m) 1.712
DRY DENSITY(Mg/m) 1.482
CONTAINER CONTAINER
CONTAINER
+ WETSOIL
CONTAINER
+ DRY SOIL DRY SOIL
MOISTURE
CONTENT
A 6.592 10.562 10.009 3.417 16.184
B 6.936 10.152 9.725 2.789 15.310
T 6.649 10.723 10.188 3.539 15.117
AVERAGE 15.537%
PERCENTAGE 21%
MOULD(Kg) 3.224
MOULD + SOIL(Kg) 5.131
COMPACTED SAMPLE(Kg) 1.907
BULK DENSITY(Mg/m) 1.907
DRY DENSITY(Mg/m) 1.578
CONTAINER CONTAINER
CONTAINER
+ WETSOIL
CONTAINER
+ DRY SOIL DRY SOIL
MOISTURE
CONTENT
A 6.781 10.908 10.162 3.381 22.064
B 6.717 12.076 11.223 4.506 18.930
T 7.272 17.051 15.318 8.046 21.539
AVERAGE 20.844%
PERCENTAGE 25%
MOULD(Kg) 3.224
MOULD + SOIL(Kg) 5.177
COMPACTED SAMPLE(Kg) 1.953
BULK DENSITY(Mg/m) 1.953
DRY DENSITY(Mg/m) 1.565
-
CONTAINER CONTAINER
CONTAINER
+ WETSOIL
CONTAINER
+ DRY SOIL DRY SOIL
MOISTURE
CONTENT
A 6.522 17.026 14.934 8.412 24.869
B 6.685 20.115 17.463 10.778 24.606
T 6.753 17.118 15.059 8.306 24.789
AVERAGE 24.755
PERCENTAGE 27%
MOULD(Kg) 3.224
MOULD + SOIL(Kg) 5.168
COMPACTED SAMPLE(Kg) 1.944
BULK DENSITY(Mg/m) 1.944
DRY DENSITY(Mg/m) 1.532
CONTAINER CONTAINER
CONTAINER
+ WETSOIL
CONTAINER
+ DRY SOIL DRY SOIL
MOISTURE
CONTENT
A 6.75 14.751 13.093 6.343 26.139
B 6.725 17.332 15.068 8.343 27.137
T 6.525 22.685 19.211 12.686 27.385
AVERAGE 26.887%
PERCENTAGE 30%
MOULD(Kg) 3.292
MOULD + SOIL(Kg) 5.211
COMPACTED SAMPLE(Kg) 1.919
BULK DENSITY(Mg/m) 1.919
DRY DENSITY(Mg/m) 1.474
CONTAINER CONTAINER
CONTAINER
+ WETSOIL
CONTAINER
+ DRY SOIL DRY SOIL
MOISTURE
CONTENT
A 6.75 14.944 13.093 6.343 29.182
B 6.725 17.628 15.068 8.343 30.684
T 6.525 23.111 19.211 12.686 30.743
AVERAGE 30.203%
-
DRY DENSITY VS MOISTURE CONTENT(MARINE CLAY)
1.46
1.48
1.5
1.52
1.54
1.56
1.58
1.6
10 15 20 25 30
%
Mg/m
White Clay
PERCENTAGE 10%
MOULD(Kg) 3.259
MOULD + SOIL(Kg) 4.733
COMPACTED
SAMPLE(Kg) 1.474
BULK DENSITY(Mg/m) 1.474
DRY DENSITY(Mg/m) 1.344
CONTAINER CONTAINER
CONTAINER
+ WETSOIL
CONTAINER
+ DRY SOIL DRY SOIL
MOISTURE
CONTENT
A 7.167 11.104 10.767 3.6 9.361
B 6.672 11.811 11.344 4.672 9.996
T 6.745 20.305 19.101 12.356 9.744
AVERAGE 9.700%
PERCENTAGE 17%
MOULD(Kg) 3.259
MOULD + SOIL(Kg) 4.962
COMPACTED
SAMPLE(Kg) 1.703
BULK DENSITY(Mg/m) 1.703
DRY DENSITY(Mg/m) 1.456
-
CONTAINER CONTAINER
CONTAINER
+ WETSOIL
CONTAINER
+ DRY SOIL DRY SOIL
MOISTURE
CONTENT
A 6.695 14.649 13.682 6.987 13.840
B 6.7 17.55 16.193 9.493 14.295
T 6.893 17.737 15.723 8.83 22.809
AVERAGE 16.981%
PERCENTAGE 20%
MOULD(Kg) 3.29
MOULD + SOIL(Kg) 5.105
COMPACTED
SAMPLE(Kg) 1.815
BULK DENSITY(Mg/m) 1.815
DRY DENSITY(Mg/m) 1.509
CONTAINER CONTAINER
CONTAINER
+ WETSOIL
CONTAINER
+ DRY SOIL DRY SOIL
MISTURE
CONTENT
A 6.783 13.338 12.308 5.525 18.643
B 6.833 13.075 11.969 5.136 21.534
T 6.868 18.51 16.523 9.655 20.580
AVERAGE 20.252%
PERCENTAGE 24%
MOULD(Kg) 3.29
MOULD + SOIL(Kg) 5.219
COMPACTED
SAMPLE(Kg) 1.929
BULK DENSITY(Mg/m) 1.929
DRY DENSITY(Mg/m) 1.555
CONTAINER CONTAINER
CONTAINER
+ WETSOIL
CONTAINER
+ DRY SOIL DRY SOIL
MOISTURE
CONTENT
A 6.799 17.246 15.298 8.499 22.920
B 6.832 22.788 19.716 12.884 23.844
T 6.998 26.796 22.796 15.798 25.320
AVERAGE 24.028%
PERCENTAGE 29%
MOULD(Kg) 3.29
MOULD + SOIL(Kg) 5.229
COMPACTED
SAMPLE(Kg) 1.939
BULK DENSITY(Mg/m) 1.939
DRY DENSITY(Mg/m) 1.508
-
CONTAINER CONTAINER
CONTAINER
+ WETSOIL
CONTAINER
+ DRY SOIL DRY SOIL
MOISTURE
CONTENT
A 18.047 37.469 33.296 15.249 27.366
B 10.195 25.937 22.472 12.277 28.224
T 9.651 38.971 32.188 22.537 30.097
AVERAGE 28.562%
PERCENTAGE 35%
MOULD(Kg) 3.259
MOULD + SOIL(Kg) 5.195
COMPACTED
SAMPLE(Kg) 1.936
BULK DENSITY(Mg/m) 1.936
DRY DENSITY(Mg/m) 1.439
CONTAINER CONTAINER
CONTAINER
+ WETSOIL
CONTAINER
+ DRY SOIL DRY SOIL
MOISTURE
CONTENT
A 10.49 31.251 26.016 15.526 33.718
B 10.155 37.04 30.072 19.917 34.985
T 9.994 43.653 34.925 24.931 35.009
AVERAGE 34.570%
PERCENTAGE 37%
MOULD(Kg) 3.259
MOULD + SOIL(Kg) 5.12
COMPACTED
SAMPLE(Kg) 1.861
BULK DENSITY(Mg/m) 1.861
DRY DENSITY(Mg/m) 1.355
CONTAINER CONTAINER
CONTAINER
+ WETSOIL
CONTAINER
+ DRY SOIL DRY SOIL
MOISTURE
CONTENT
A 27.683 54.717 47.466 19.783 36.653
B 10.282 57.84 44.922 34.64 37.292
T 7.078 45.833 35.128 28.05 38.164
AVERAGE 37.370%
-
DRY DENSITY VS MOISTURE CONTENT(WHITE CLAY)
1.3
1.35
1.4
1.45
1.5
1.55
1.6
5 10 15 20 25 30 35 40
%
Mg/m
White Kaolin
PERCENTAGE 11%
MOULD(Kg) 3.17
MOULD + SOIL(Kg) 4.61
COMPACTED
SAMPLE(Kg) 1.44
BULK DENSITY(Mg/m) 1.44
DRY DENSITY(Mg/m) 1.300
CONTAINER CONTAINER
CONTAINER
+ WETSOIL
CONTAINER
+ DRY SOIL DRY SOIL
MOISTURE
CONTENT
A 7.17 24.937 23.178 16.008 10.988
B 6.809 26.647 24.755 17.946 10.543
T 6.897 26.643 24.715 17.818 10.821
AVERAGE 10.784%
-
PERCENTAGE 15%
MOULD(Kg) 3.17
MOULD + SOIL(Kg) 4.85
COMPACTED
SAMPLE(Kg) 1.68
BULK DENSITY(Mg/m) 1.68
DRY DENSITY(Mg/m) 1.461
CONTAINER CONTAINER
CONTAINER
+ WETSOIL
CONTAINER
+ DRY SOIL DRY SOIL
MOISTURE
CONTENT
A 6.956 23.981 21.8 14.844 14.693
B 6.811 28.888 25.951 19.14 15.345
T 6.758 27.503 24.802 18.044 14.969
AVERAGE 15.002%
PERCENTAGE 20%
MOULD(Kg) 3.17
MOULD + SOIL(Kg) 4.95
COMPACTED
SAMPLE(Kg) 1.78
BULK DENSITY(Mg/m) 1.78
DRY DENSITY(Mg/m) 1.489
CONTAINER CONTAINER
CONTAINER
+ WETSOIL
CONTAINER
+ DRY SOIL DRY SOIL
MOISTURE
CONTENT
A 6.864 46.592 40.136 33.272 19.404
B 6.826 40.688 35.128 28.302 19.645
T 6.819 45.734 39.333 32.514 19.687
AVERAGE 19.579%
PERCENTAGE 24%
MOULD(Kg) 3.17
MOULD + SOIL(Kg) 4.95
COMPACTED
SAMPLE(Kg) 1.78
BULK DENSITY(Mg/m) 1.78
DRY DENSITY(Mg/m) 1.432
CONTAINER CONTAINER
CONTAINER
+ WETSOIL
CONTAINER
+ DRY SOIL DRY SOIL
MOISTURE
CONTENT
A 18.038 43.149 38.251 20.213 24.232
B 6.786 51.227 42.47 35.684 24.540
T 9.571 44.471 37.703 28.132 24.058
AVERAGE 24.277%
-
PERCENTAGE 30%
MOULD(Kg) 3.17
MOULD + SOIL(Kg) 5.1
COMPACTED
SAMPLE(Kg) 1.93
BULK DENSITY(Mg/m) 1.93
DRY DENSITY(Mg/m) 1.485
CONTAINER CONTAINER
CONTAINER
+ WETSOIL
CONTAINER
+ DRY SOIL DRY SOIL
MOISTURE
CONTENT
A 9.571 33.077 27.644 18.073 30.061
B 10.156 42.222 34.845 24.689 29.880
T 9.719 48.445 39.522 29.803 29.940
AVERAGE 29.960%
PERCENTAGE 37%
MOULD(Kg) 3.17
MOULD + SOIL(Kg) 4.96
COMPACTED
SAMPLE(Kg) 1.79
BULK DENSITY(Mg/m) 1.79
DRY DENSITY(Mg/m) 1.310
CONTAINER CONTAINER
CONTAINER
+ WETSOIL
CONTAINER
+ DRY SOIL DRY SOIL
MOISTURE
CONTENT
A 9.99 42.516 34.092 24.102 34.951
B 6.921 44.01 33.405 26.484 40.043
T 6.73 31.047 24.772 18.042 34.780
AVERAGE 36.591%
-
DRY DENSITY VS MOISTURE CONTENT(KAOLIN)
1.25
1.3
1.35
1.4
1.45
1.5
5 10 15 20 25 30 35 40
Moisture Content(%)
Dry
Density(M
g/m
)
-
APPENDIX B
Data for Vane Shear Test
Marine Clay
Mass of mould+compacted
soil(kg) 9.780 mass of container(g) 6.888
Mass of mould(kg) 5.619
mass of container+wet
soil(g) 17.512
mass of compacted
sample(kg) 4.161
mass of container+dry
soil(g) 15.715
bulk density(Mg/m) 1.806 mass of dry soil(g) 8.827
dry density(Mg/m) 1.500 moisture content (%) 20.358
FRACTION TNH & BESI 84
FRACTION TNH & BILAH 22
FACTOR 2
UNDRAINED SHEAR STRENGTH(kPa) 146
Mass of mould+compacted
soil(kg) 9.977 mass of container(g) 7.062
Mass of mould(kg) 5.619
mass of container+wet
soil(g) 22.858
mass of compacted
sample(kg) 4.358
mass of container+dry
soil(g) 19.908
bulk density(Mg/m) 1.891 mass of dry soil(g) 12.846
dry density(Mg/m) 1.538 moisture content (%) 22.964
FRACTION TNH & BESI 62
FRACTION TNH & BILAH 13
FACTOR 2
UNDRAINED SHEAR STRENGTH(kPa) 111
-
Marine Clay
Mass of mould+compacted
soil(kg) 10.040 mass of container(g) 6.844
Mass of mould(kg) 5.622
mass of container+wet
soil(g) 22.307
mass of compacted
sample(kg) 4.418
mass of container+dry
soil(g) 18.990
bulk density(Mg/m) 1.917 mass of dry soil(g) 12.146
dry density(Mg/m) 1.506 moisture content (%) 27.309
FRACTION TNH & BESI 40
FRACTION TNH & BILAH 4
FACTOR 2
UNDRAINED SHEAR STRENGTH(kPa) 76
Mass of mould+compacted
soil(kg) 10.032 mass of container(g) 6.959
Mass of mould(kg) 5.622
mass of container+wet
soil(g) 25.999
mass of compacted
sample(kg) 4.410
mass of container+dry
soil(g) 21.602
bulk density(Mg/m) 1.914 mass of dry soil(g) 14.643
dry density(Mg/m) 1.472 moisture content (%) 30.028
FRACTION TNH & BESI 26
FRACTION TNH & BILAH 2
FACTOR 2
UNDRAINED SHEAR STRENGTH(kPa) 50
-
White Clay
Mass of mould+compacted
soil(kg) 9.897 mass of container(g) 6.781
Mass of mould(kg) 5.622
mass of container+wet
soil(g) 16.688
mass of compacted
sample(kg) 4.275
mass of container+dry
soil(g) 14.386
bulk density(Mg/m) 1.855 mass of dry soil(g) 7.605
dry density(Mg/m) 1.424 moisture content (%) 30.270
FRACTION TNH & BESI 54
FRACTION TNH & BILAH 7.5
FACTOR 2
UNDRAINED SHEAR STRENGTH(kPa) 100.5
Mass of mould+compacted
soil(kg) 9.906 mass of container(g) 6.943
Mass of mould(kg) 5.622
mass of container+wet
soil(g) 20.792
mass of compacted
sample(kg) 4.284
mass of container+dry
soil(g) 17.354
bulk density(Mg/m) 1.859 mass of dry soil(g) 10.411
dry density(Mg/m) 1.397 moisture content (%) 33.023
FRACTION TNH & BESI 25
FRACTION TNH & BILAH 4
FACTOR 2
UNDRAINED SHEAR STRENGTH(kPa) 46
-
White Clay
Mass of mould+compacted
soil(kg) 9.930 mass of container(g) 10.243
Mass of mould(kg) 5.622
mass of container+wet
soil(g) 25.714
mass of compacted
sample(kg) 4.308
mass of container+dry
soil(g) 21.525
bulk density(Mg/m) 1.869 mass of dry soil(g) 11.282
dry density(Mg/m) 1.363 moisture content (%) 37.130
FRACTION TNH & BESI 16
FRACTION TNH & BILAH 2
FACTOR 2
UNDRAINED SHEAR STRENGTH(kPa) 30
Mass of mould+compacted
soil(kg) 9.934 mass of container(g) 6.523
Mass of mould(kg) 5.622
mass of container+wet
soil(g) 15.131
mass of compacted
sample(kg) 4.312
mass of container+dry
soil(g) 12.671
bulk density(Mg/m) 1.871 mass of dry soil(g) 6.148
dry density(Mg/m) 1.336 moisture content (%) 40.013
FRACTION TNH & BESI 12
FRACTION TNH & BILAH 0.5
FACTOR 2
UNDRAINED SHEAR STRENGTH(kPa) 23.5
-
White Kaolin
Mass of mould+compacted
soil(kg) 9.887 mass of container(g) 6.781
Mass of mould(kg) 5.619
mass of container+wet
soil(g) 14.237
mass of compacted
sample(kg) 4.268
mass of container+dry
soil(g) 12.725
bulk density(Mg/m) 1.852 mass of dry soil(g) 5.944
dry density(Mg/m) 1.476 moisture content (%) 25.437
FRACTION TNH & BESI 52
FRACTION TNH & BILAH 6
FACTOR 2
UNDRAINED SHEAR STRENGTH(kPa) 98
Mass of mould+compacted
soil(kg) 9.807 mass of container(g) 6.593
Mass of mould(kg) 5.619
mass of container+wet
soil(g) 23.636
mass of compacted
sample(kg) 4.188
mass of container+dry
soil(g) 19.698
bulk density(Mg/m) 1.817 mass of dry soil(g) 13.105
dry density(Mg/m) 1.397 moisture content (%) 30.050
FRACTION TNH & BESI 18
FRACTION TNH & BILAH 2
FACTOR 2
UNDRAINED SHEAR STRENGTH(kPa) 34
-
White Kaolin
Mass of mould+compacted
soil(kg) 9.839 mass of container(g) 6.806
Mass of mould(kg) 5.620
mass of container+wet
soil(g) 24.564
mass of compacted
sample(kg) 4.219
mass of container+dry
soil(g) 19.996
bulk density(Mg/m) 1.831 mass of dry soil(g) 13.190
dry density(Mg/m) 1.360 moisture content (%) 34.632
FRACTION TNH & BESI 6
FRACTION TNH & BILAH 0
FACTOR 2
UNDRAINED SHEAR STRENGTH(kPa) 12
Mass of mould+compacted
soil(kg) 9.800 mass of container(g) 7.008
Mass of mould(kg) 5.619
mass of container+wet
soil(g) 30.923
mass of compacted
sample(kg) 4.181
mass of container+dry
soil(g) 24.072
bulk density(Mg/m) 1.814 mass of dry soil(g) 17.064
dry density(Mg/m) 1.295 moisture content (%) 40.149
FRACTION TNH & BESI 3
FRACTION TNH & BILAH 0
FACTOR 2
UNDRAINED SHEAR STRENGTH(kPa) 6
-
APPENDIX C
Data for CBR test
Marine Clay
Mould+compacted soil(kg) 9.767 Mass of container(g) 9.799
Mass of mould(kg) 5.612 Container+wet soil(g) 19.573
Mass of compacted sample(kg) 4.155 Container+dry soil(g) 17.943
Bulk density(Mg/m) 1.803 Mass of dry soil(g) 8.144
Dry density(Mg/m) 1.502 Moisture content(%) 20.015
gauge reading(div) force(kN)
penetration(mm) top bottom top bottom
0.000 0.000 0.000 0.000 0.000
0.250 54.000 110.000 0.184 0.374
0.500 98.000 195.000 0.333 0.663
0.750 171.000 265.000 0.581 0.901
1.000 227.000 330.000 0.772 1.122
1.250 270.000 385.000 0.918 1.309
1.500 302.000 435.000 1.027 1.479
1.750 333.000 475.000 1.132 1.615
2.000 364.000 510.000 1.238 1.734
2.250 393.000 543.000 1.336 1.846
2.500 422.000 570.000 1.435 1.938
2.750 441.000 596.000 1.499 2.026
3.000 469.000 619.000 1.595 2.105
3.250 494.000 640.000 1.680 2.176
3.500 519.000 658.000 1.765 2.237
3.750 539.000 674.000 1.833 2.292
4.000 558.000 688.000 1.897 2.339
4.250 576.000 703.000 1.958 2.390
4.500 593.000 717.000 2.016 2.438
4.750 610.000 731.000 2.074 2.485
5.000 628.000 744.000 2.135 2.530
5.250 644.000 756.000 2.190 2.570
5.500 660.000 769.000 2.244 2.615
5.750 676.000 779.000 2.298 2.649
6.000 693.000 790.000 2.356 2.686
6.250 708.000 799.000 2.407 2.717
6.500 723.000 808.000 2.458 2.747
6.750 737.000 817.000 2.506 2.778
7.000 753.000 826.000 2.560 2.808
7.250 765.000 834.000 2.601 2.836
7.500 779.000 841.000 2.649 2.859
-
Marine Clay
Mould+compacted soil(kg) 9.990 Mass of container(g) 9.109
Mass of mould(kg) 5.612 Container+wet soil(g) 25.461
Mass of compacted sample(kg) 4.378 Container+dry soil(g) 22.404
Bulk density(Mg/m) 1.900 Mass of dry soil(g) 13.295
Dry density(Mg/m) 1.545 Moisture content(%) 22.994
gauge reading(div) force(kN)
penetration(mm) top bottom top bottom
0.000 0.000 0.000 0.000 0.000
0.250 19.000 43.000 0.065 0.146
0.500 32.000 79.000 0.109 0.269
0.750 47.000 129.000 0.160 0.439
1.000 63.000 180.000 0.214 0.612
1.250 77.000 214.000 0.262 0.728
1.500 91.000 245.000 0.309 0.833
1.750 105.000 273.000 0.357 0.928
2.000 119.000 296.000 0.405 1.006
2.250 136.000 318.000 0.462 1.081
2.500 150.000 337.000 0.510 1.146
2.750 165.000 355.000 0.561 1.207
3.000 181.000 372.000 0.615 1.265
3.250 196.000 388.000 0.666 1.319
3.500 212.000 400.000 0.721 1.360
3.750 228.000 413.000 0.775 1.404
4.000 244.000 425.000 0.830 1.445
4.250 261.000 436.000 0.887 1.482
4.500 275.000 447.000 0.935 1.520
4.750 290.000 457.000 0.986 1.554
5.000 305.000 466.000 1.037 1.584
5.250 319.000 475.000 1.085 1.615
5.500 336.000 485.000 1.142 1.649
5.750 351.000 493.000 1.193 1.676
6.000 366.000 501.000 1.244 1.703
6.250 379.000 509.000 1.289 1.731
6.500 392.000 517.000 1.333 1.758
6.750 404.000 524.000 1.374 1.782
7.000 416.000 533.000 1.414 1.812
7.250 426.000 540.000 1.448 1.836
7.500 436.000 547.000 1.482 1.860
-
Marine Clay
Mould+compacted soil(kg) 10.012 Mass of container(g) 9.794
Mass of mould(kg) 5.612 Container+wet soil(g) 25.287
Mass of compacted sample(kg) 4.400 Container+dry soil(g) 22.027
Bulk density(Mg/m) 1.909 Mass of dry soil(g) 12.233
Dry density(Mg/m) 1.508 Moisture content(%) 26.649
gauge reading(div) force(kN)
penetration(mm) top bottom top bottom
0.000 0.000 0.000 0.000 0.000
0.250 17.000 29.000 0.058 0.099
0.500 25.000 43.000 0.085 0.146
0.750 33.000 54.000 0.112 0.184
1.000 40.000 65.000 0.136 0.221
1.250 45.000 73.000 0.153 0.248
1.500 53.000 81.000 0.180 0.275
1.750 58.000 88.000 0.197 0.299
2.000 63.000 96.000 0.214 0.326
2.250 69.000 102.000 0.235 0.347
2.500 74.000 109.000 0.252 0.371
2.750 78.000 114.000 0.265 0.388
3.000 83.000 120.000 0.282 0.408
3.250 88.000 125.000 0.299 0.425
3.500 94.000 130.000 0.320 0.442
3.750 97.000 135.000 0.330 0.459
4.000 101.000 140.000 0.343 0.476
4.250 106.000 145.000 0.360 0.493
4.500 109.000 150.000 0.371 0.510
4.750 113.000 154.000 0.384 0.524
5.000 118.000 158.000 0.401 0.537
5.250 121.000 162.000 0.411 0.551
5.500 125.000 166.000 0.425 0.564
5.750 129.000 170.000 0.439 0.578
6.000 134.000 174.000 0.456 0.592
6.250 137.000 177.000 0.466 0.602
6.500 141.000 181.000 0.479 0.615
6.750 145.000 184.000 0.493 0.626
7.000 148.000 188.000 0.503 0.639
7.250 152.000 191.000 0.517 0.649
7.500 155.000 194.000 0.527 0.660
-
Marine Clay
Mould+compacted soil(kg) 9.767 Mass of container(g) 9.799
Mass of mould(kg) 5.612 Container+wet soil(g) 19.573
Mass of compacted sample(kg) 4.155 Container+dry soil(g) 17.943
Bulk density(Mg/m) 1.803 Mass of dry soil(g) 8.144
Dry density(Mg/m) 1.502 Moisture content(%) 20.015
gauge reading(div) force(kN)
penetration(mm) top bottom top bottom
0.000 0.000 0.000 0.000 0.000
0.250 54.000 110.000 0.184 0.374
0.500 98.000 195.000 0.333 0.663
0.750 171.000 265.000 0.581 0.901
1.000 227.000 330.000 0.772 1.122
1.250 270.000 385.000 0.918 1.309
1.500 302.000 435.000 1.027 1.479
1.750 333.000 475.000 1.132 1.615
2.000 364.000 510.000 1.238 1.734
2.250 393.000 543.000 1.336 1.846
2.500 422.000 570.000 1.435 1.938
2.750 441.000 596.000 1.499 2.026
3.000 469.000 619.000 1.595 2.105
3.250 494.000 640.000 1.680 2.176
3.500 519.000 658.000 1.765 2.237
3.750 539.000 674.000 1.833 2.292
4.000 558.000 688.000 1.897 2.339
4.250 576.000 703.000 1.958 2.390
4.500 593.000 717.000 2.016 2.438
4.750 610.000 731.000 2.074 2.485
5.000 628.000 744.000 2.135 2.530
5.250 644.000 756.000 2.190 2.570
5.500 660.000 769.000 2.244 2.615
5.750 676.000 779.000 2.298 2.649
6.000 693.000 790.000 2.356 2.686
6.250 708.000 799.000 2.407 2.717
6.500 723.000 808.000 2.458 2.747
6.750 737.000 817.000 2.506 2.778
7.000 753.000 826.000 2.560 2.808
7.250 765.000 834.000 2.601 2.836
7.500 779.000 841.000 2.649 2.859
-
Marine Clay
Mould+compacted soil(kg) 10.103 Mass of container(g) 9.899
Mass of mould(kg) 5.612 Container+wet soil(g) 28.427
Mass of compacted sample(kg) 4.491 Container+dry soil(g) 24.119
Bulk density(Mg/m) 1.949 Mass of dry soil(g) 14.220
Dry density(Mg/m) 1.496 Moisture content(%) 30.295
gauge reading(div) force(kN)
penetration(mm) top bottom top bottom
0.000 0.000 0.000 0.000 0.000
0.250 4.000 15.000 0.014 0.051
0.500 8.000 18.000 0.027 0.061
0.750 11.000 21.000 0.037 0.071
1.000 14.000 24.000 0.048 0.082
1.250 17.000 26.000 0.058 0.088
1.500 20.000 31.000 0.068 0.105
1.750 22.500 34.000 0.077 0.116
2.000 25.000 37.000 0.085 0.126
2.250 28.000 39.500 0.095 0.134
2.500 31.000 43.000 0.105 0.146
2.750 34.000 46.000 0.116 0.156
3.000 37.000 49.000 0.126 0.167
3.250 40.000 52.000 0.136 0.177
3.500 43.000 55.000 0.146 0.187
3.750 46.000 58.000 0.156 0.197
4.000 49.000 62.000 0.167 0.211
4.250 52.000 64.000 0.177 0.218
4.500 54.000 66.000 0.184 0.224
4.750 56.000 68.000 0.190 0.231
5.000 58.000 70.000 0.197 0.238
5.250 60.000 73.000 0.204 0.248
5.500 63.000 75.000 0.214 0.255
5.750 65.000 77.000 0.221 0.262
6.000 67.000 79.000 0.228 0.269
6.250 69.000 81.000 0.235 0.275
6.500 71.000 83.000 0.241 0.282
6.750 73.000 85.000 0.248 0.289
7.000 75.000 87.000 0.255 0.296
7.250 77.000 89.000 0.262 0.303
7.500 79.000 91.000 0.269 0.309
-
White Clay
Mould+compacted soil(kg) 9.891 Mass of container(g) 6.959
Mass of mould(kg) 5.619 Container+wet soil(g) 25.999
Mass of compacted sample(kg) 4.272 Container+dry soil(g) 21.602
Bulk density(Mg/m) 1.854 Mass of dry soil(g) 14.643
Dry density(Mg/m) 1.426 Moisture content(%) 30.028
gauge reading(div) force(kN)
penetration(mm) top bottom top bottom
0.000 0.000 0.000 0.000 0.000
0.250 7.000 12.000 0.043 0.073
0.500 13.000 26.000 0.079 0.159
0.750 19.000 40.000 0.116 0.244
1.000 25.000 50.000 0.153 0.305
1.250 32.000 60.000 0.195 0.366
1.500 37.000 69.000 0.226 0.421
1.750 43.000 77.000 0.262 0.470
2.000 49.000 85.000 0.299 0.519
2.250 55.000 92.000 0.336 0.561
2.500 60.000 98.000 0.366 0.598
2.750 66.000 104.000 0.403 0.634
3.000 72.000 109.000 0.439 0.665
3.250 77.000 115.000 0.470 0.702
3.500 83.000 121.000 0.506 0.738
3.750 89.000 127.000 0.543 0.775
4.000 94.000 133.000 0.573 0.811
4.250 100.000 138.000 0.610 0.842
4.500 106.000 143.000 0.647 0.872
4.750 111.000 149.000 0.677 0.909
5.000 116.000 154.000 0.708 0.939
5.250 120.000 159.000 0.732 0.970
5.500 126.000 164.000 0.769 1.000
5.750 130.000 168.000 0.793 1.025
6.000 136.000 173.000 0.830 1.055
6.250 142.000 177.000 0.866 1.080
6.500 146.000 182.000 0.891 1.110
6.750 150.000 185.